2009
DOI: 10.1016/j.jhydrol.2009.02.014
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Benzene dispersion and natural attenuation in an alluvial aquifer with strong interactions with surface water

Abstract: This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their pe… Show more

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Cited by 25 publications
(13 citation statements)
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References 37 publications
(41 reference statements)
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“…The required parameters are shown in Table . The aquifer hydraulic conductivity and porosity ranges were based on previous studies at the field site [ Batlle‐Aguilar , ; Batlle‐Aguilar et al ., ] and are consistent with other studies conducted elsewhere in the same alluvial aquifer [ Brouyère , ; Wildemeersch et al ., ]. The density, specific heat capacity and thermal conductivity of water are fixed at 1000 kg m −3 , 4185 J kg −1 °C −1 , and 0.5 W m −1 °C −1 .…”
Section: Methodssupporting
confidence: 92%
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“…The required parameters are shown in Table . The aquifer hydraulic conductivity and porosity ranges were based on previous studies at the field site [ Batlle‐Aguilar , ; Batlle‐Aguilar et al ., ] and are consistent with other studies conducted elsewhere in the same alluvial aquifer [ Brouyère , ; Wildemeersch et al ., ]. The density, specific heat capacity and thermal conductivity of water are fixed at 1000 kg m −3 , 4185 J kg −1 °C −1 , and 0.5 W m −1 °C −1 .…”
Section: Methodssupporting
confidence: 92%
“…Groundwater head in monitored wells follows similar fluctuations as the river, with amplitudes progressively attenuated and time lags increased at the wells farther from the river (Figure b). Under base flow conditions (river level at 59.4 m asl) the aquifer discharges into the Meuse River, but the hydraulic gradient is reversed when the river level rises beyond approximately 60.3 m asl, causing surface water to infiltrate into the alluvial aquifer at the study site [ Batlle‐Aguilar et al ., ].…”
Section: Study Sitementioning
confidence: 99%
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“…Their high concentrations (exceeding respectively 15.7 and 0.39 mg/dm 3 ) can be explained by high solubility of these compounds in water. Comparable and even higher exceeding of allowable concentrations of these compounds was noted in the 1990s on the area of petrol station [1,2]. Increased amounts (exceeding 100 µg/dm 3 ) were noted as well in the case of styrene, 1,3,5-trimethylbenzene, 4-isopropylbenzene, n-butylbenzene and tert-butylbenzene with 1,2,4-trimerthylbenzene.…”
Section: Resultsmentioning
confidence: 92%